Title: Sea Floor Spreading
1Sea Floor Spreading
- EQ What is the process of sea-floor spreading?
2Mid-Ocean Ridge
- Mid-Ocean Ridge The undersea mountain chain
where new ocean floor is produced a divergent
plate boundary
3Mid Ocean Ridge
4 Sonar
- Sonar A device that determines the distance of
an object under water by recording echoes of
sound waves
5The sonar is used to map the ocean floor
- Sonar bounces sound waves off underwater objects
and then records the echoes of these sound waves - The time it takes for the echo to arrive
indicates the distance to the object
6Evidence for Sea-Floor Spreading
In the 1960s, Harry Hess examined maps of the mid
ocean ridge. He proposed that the ocean floors
move like conveyor belts, carrying the continents
with them.
7Sea-Floor Spreading
- The process by which molten material adds new
oceanic crust to the ocean floor
8 What evidence did scientists find for sea-floor
spreading in the 1960s?
- Evidence from molten material
- Evidence from magnetic stripes
- Evidence from drilling samples
9Evidence From Molten Material
- Alvins crew found strange rocks shaped like
pillows or like toothpaste squeezed from a tube - Such rocks can form only when molten material
hardens quickly after erupting under water - The presence of these rocks showed that molten
material has erupted again and again from cracks
along the central valley of the mid-ocean ridge. - http//www.pmel.noaa.gov/vents/nemo/explorer/conce
pts/pillow_lava.html
10- Scientists discovered that the rock that makes up
the ocean floor lies in a pattern of magnetized
stripes - 780,000 years ago, magnetic poles reversed
themselves - If they reversed today, the needle in a compass
would point south instead of north - The rock in the ocean is made of iron, which
began as molten material
Evidence From Magnetic Stripes
11Evidence From Drilling Samples
- When scientists sampled the rocks, they found
that the further away from the ridge the rocks
were the older they were - The younger rocks were always in the center of
the ridges
12Subduction at Deep-Ocean Trenches
13Deep-Ocean Trenches
- A deep valley along the ocean floor through which
oceanic crust slowly sinks towards the mantle
14Subduction
- Subduction The process by which oceanic crust
sinks through a deep-ocean trench and back into
the mantle a convergent plate boundary
15Guide For Reading What happens to the ocean
floor at deep ocean trenches?
- At deep-ocean trenches, two plates collide
causing the denser of the two plates to dive back
to the mantle. This process is known as
subduction. - Over tens of million of years, this material
melts back into molten material and may rise
again as new oceanic crust.
16Guide For Reading What is the process of
sea-floor spreading?
- At the mid-ocean ridge, molten material rises
from the mantle and erupts. The molten material
then spreads out, pushing older rock to both
sides of the ridge. - Over tens of millions of years, the process
continues until the oldest ocean floor collides
with the continental crust - The more dense oceanic crust subducts (sinks)
back into the mantle at a deep-ocean trench
17Subduction and Earths Oceans
18Subduction in the Pacific Ocean
- Subduction in the Pacific Ocean is occurring at a
greater rate than sea-floor is expanding - This is caused by the large amount of trenches
19Subduction in the Atlantic
- The Atlantic Ocean is expanding at a greater rate
than subducting - This is because of the low number of trenches in
the Atlantic - Over time the entire ocean gets larger and pushes
against the continents
20Class Work and Homework
- Fill In
- What did I learn
- Confused
- Say
- Carefully read pages F33 F39, Answer questions
1-5 on page F39